A&A 373, 816-826 (2001)
DOI: 10.1051/0004-6361:20010651
R. Srianand1 - P. Petitjean 2,3
1 -
IUCAA, Post Bag 4, Ganeshkhind, Pune 411 007, India
2 -
Institut d'Astrophysique de Paris - CNRS, 98bis Boulevard
Arago, 75014 Paris, France
3 -
UA CNRS 173 - DAEC, Observatoire de Paris-Meudon, 92195 Meudon
Cedex, France
Received 6 February 2001 / Accepted 23 April 2001
Abstract
We report the detection of a Broad Absorption Line (BAL) outflow
in the spectrum of the
(Mg II) = 2.201 QSO Tol 1037-2703
with three main BALs at 36000, 25300 and 22300 km s-1 outflow velocities.
Although the overall flow is dominated by high ionization lines
like N V and C IV, the gas of highest velocity shows absorption from
Mg I, Mg II and Fe II.
Covering factor arguments suggest that the absorbing complexes are
physically associated with the QSO and have transverse dimensions
smaller than that of the UV continuum emitting region
(r < 0.1 pc). We show that the C IV absorption at
= 2.082 has a covering factor
0.86 and the
absorption profile has varied over the last four years. The detection
of absorption from excited fine structure levels of C II and
Si II in narrow components embedded in the C IV trough
reveals large density inhomogeneities. IR pumping is the most likely
excitation process.
The
= 2.139 system is a moderately damped Lyman-
system
with log N(H I)
19.7. The weakness of the metal lines
together with the high quality of the data make the metallicity
measurements particularly reliable. The absolute metallicity is close
to solar with [Zn/H] = -0.26. The
-chain elements have
metallicities consistently solar (respectively +0.05, -0.02, -0.03
and -0.15 for [Mg/H], [Si/H], [P/H] and [S/H]) and iron peak
elements are depleted by a factor of about two ([Fe/Zn], [Cr/Zn],
[Mn/Zn] and [Ni/Zn] are equal to -0.39, -0.27, -0.49,
-0.30). Lines from C I are detected but H2 is absent with a
molecular to neutral hydrogen fraction less than
8
10-6. From the ionization state of the gas, we argue
that the system is situated
few Mpc away from the QSO. High
metallicity and low nitrogen abundance, [N/Zn] = -1.40, favor the
idea that metals have been released by massive stars during a
starburst of less than 0.5 Gyr of age.
Using the upper
limit on the C I* column density in two components, we obtain
upper limits on the background temperature of 16.2 and 13.2 K respectively.
Key words: galaxies: intergalactic medium - galaxies: quasars: absorption lines
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Figure 1:
Portion of the Tol 1037-2703 spectrum.
A high-quality UVES spectrum of Q1101-264 shifted in wavelength and
intensity is overplotted (dotted line).
Position of various BALs discussed in the text are indicated.
The subscripts "A'', "B'' and "C'' denote the
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The remarkable similarity of four C IV absorption systems at redshift
1.95 <
< 2.14 in the spectra of Tol 1037-2703 (
= 2.20)
and 1038-2712 (
= 2.33) separated by only 17.9 arcmin on the sky has
created considerable interest in the past. However the nature and origin
of these common absorption systems are still unclear.
There are arguments as well as counter arguments
for (i) the absorption being produced by a super-cluster sitting in
front of the two quasars and (ii) part of the systems being intrinsically
associated with the QSOs (see Jakobsen et al. 1986; Ulrich & Perryman 1986;
Cristiani et al. 1987; Robertson 1987; Sargent & Steidel 1987; Dinshaw & Impey 1996; Lespine & Petitjean 1997).
Here we use a high resolution and high S/N ratio spectrum of Tol 1037-2703
of quality an order of magnitude higher than previous data to investigate the
nature of the systems close to the quasar redshift, mainly the broad outflow
and the systems at
2.082 and 2.139. As it is now established that the
absorbing gas physically associated with the QSOs often shows some or all of:
(i) partial coverage, (ii) excited fine-structure lines, (iii) time
variability, (iv) broader albeit smoother profile, (v) high metal enrichment
(see e.g. Petitjean et al. 1994; Hamann 1997; Petitjean & Srianand 1999;
Srianand & Petitjean 2000), we can investigate the nature of these systems
using these indicators.
Observations are described in Sect. 2. Section 3 presents the spectral
energy distribution and accurate redshift of the QSO. We discuss the BAL flow
in Sect. 4 and study the nature of the
2.082 and 2.139 C IV
systems in
greater detail in Sect. 5. The results are summarized and discussed in
Sect. 6.
The Ultra-violet and Visible Echelle Spectrograph (D'Odorico et al. 2000)
mounted on the ESO Kueyen 8.2 m telescope at the Paranal observatory
was used on April 5 to 8, 2000 to obtain high-spectral
resolution spectra of Tol 1037-2703. The slit width was 1 arcsec (the seeing
FWHM was most of the time better than 0.8 arcsec) and the CCDs were binned
2
2 resulting in a resolution of
45000. The total exposure time
9 hours was split into 1 h exposures. The data were reduced in the
dedicated context of MIDAS, the ESO data reduction package, using the UVES
pipeline in an interactive mode. The main characteristics of the pipeline are
to perform a precise inter-order background subtraction for science frames and
master flat-fields, and an optimal extraction of the object signal rejecting
cosmic ray impacts and subtracting the sky at the same time.
The reduction is checked step by step. Wavelengths were corrected to
vacuum-heliocentric values and individual 1D spectra were combined together.
The resulting S/N ratio per pixel is of the order of 20 at
3500 Å
and 40 at
6000 Å.
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Figure 2:
The Mg II emission line of Tol 1037-2703
at a redshift of z = 2.201.
The vertical dotted line marks the expected position the emission line for the
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Unlike most of the other emission lines, Mg II emission is
clearly seen in our red spectrum (see Fig. 2). This provides
us with the accurate measurement of the emission redshift of the QSO,
= 2.201, which is important for the study of associated
systems. Jakobsen et al. (1986) have measured
= 2.193
from the high excitation emission lines, which is 2400 km s-1smaller than our determination. Gaskell (1982) has shown, however,
that there is a systematic difference between the redshifts derived
from broad emission-lines of
different ionization levels. The mean blue-shift
of C IV, N V and possibly Lyman-
with respect to
low-ionization lines as O I, Mg II and the Balmer lines is about
600 km s-1 (Espey et al. 1989). The corresponding blueshift for
Tol 1037-2703 is larger than this but not exceptional.
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Figure 3:
Velocity plot of broad absorption lines from
the
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The so-called low ionization Mg II BALs are seen in 15% of the
BALQSOs detected in optical surveys (Voit et al. 1993). All the
known Mg II BAL systems have strong absorption due to C IV, Al II and
Al III; the absorption due to Al III being prominent compared to that of
Al II. The profiles of low ionization BALs are always shallower and
narrower than that of high ionization transitions (Voit et al.
1993). Becker et al. (2000) have suggested that the fraction of
BALs amongst radio selected QSOs are high and
50% of them show
absorption due to low ionization species. It is interesting to
note that no BAL due to Mg I has been mentioned up to now
(see however de Kool et al. 2001).
After carefully taking into account the atmospheric features, the
Mg I
2852
rest equivalent width is
Å and
FWHM= 1523 km s-1.
Correspondingly,
(Mg II) is 2.35 Å. This
gives N(Mg II)
and N(Mg I)
cm-2.
As the ionization potential of Mg I is less than 13.6 eV,
even if hydrogen is completely neutral, N(Mg II) is expected
and observed to be larger than N(Mg I). This strongly suggests that
the absorbing gas does not completely cover the background source. From the
residual intensities we estimate that the covering factor could be
as low as
0.1 which would be consistent with the strength of the
Fe II lines.
The Mg II absorption is redshifted in a region devoid of any
emission line. This means the absorbing gas has a projected size
of less than 0.01 pc (10% of the typical size of the UV continuum emitting
region). It must be noted that the presence of such low covering
factor in BAL flows has already been mentioned (Hamann
et al. 1997; Telfer et al. 1998; Srianand & Petitjean 2000).
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Figure 4:
Velocity plot of broad absorption lines in the twin
BAL system at
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Figure 5:
Velocity plot of high ionization lines from
the
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The absence of absorption due to singly ionized species, the weakness of the
H I Lyman-
line and the fact that N V is stronger than
C IV suggest that ionization conditions in these systems are similar
to those of standard high-ionization BALs. Assuming the nitrogen abundance
to be ten times solar and N V to be the dominant nitrogen species we estimate
a lower limit on the total hydrogen column density of 3.9
and 4.2
for the two components.
The observed upper limit on N(H I) at
= 1.7018
is 10
implying log
(Hamann 1997).
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Figure 6:
Velocity plot of low ionization lines from
the
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This component also shows absorption due to low ionization lines such as
Al II, Si II, C II, Si III, Al III and
absorption due to fine-structure lines of Si II and C II (see
Fig. 6). The expected position of Mg II
2797
unfortunately coincides with a small gap in our UVES spectrum. The detected
low ionization lines have a complex structure with a strong narrow component
at
superimposed on a diffuse broader profile.
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Figure 7:
Covering factor estimated from the C IV absorption at
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(1) |
The estimated covering factor for C IV is constant within the absorption line
profile. This suggests that there are no large variations of the
line of sight velocity field across the absorbing cloud. The estimated
covering factor for the component at
km s-1 (i.e.
4754 Å) is
.
The distinct narrow component
in the red wing showing complete coverage probably corresponds to a normal
intervening system.
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Figure 8:
Covering factor estimated from the Al III absorption at
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The same analysis is done for the Al III doublet (see Fig. 8)
which is not contaminated by any broad absorption trough.
In this wavelength range too, the continuum is well approximated by
spline fitting.
As discussed before, the profile shows a narrow component on top of a broad
absorption structure. Within the uncertainties, the covering factor
is in the range
0.2-0.3 (see Fig. 8). It is well known,
however, that the blending of weak unresolved lines can mimic partial coverage
(Lespine & Petitjean 1997). In order to ascertain the above result, we
have fitted the Al III doublet with multiple Voigt profile components
taking into account the partial coverage.
The best fit result is presented in Fig. 9. It is apparent from the
figure that, at least for the strongest component, partial covering factor
(
0.3) is needed. This confirms that the gas responsible for
the
= 2.082 system covers the background source only partially. The
estimated covering factor varies from one species to the other, being larger
for higher excitation lines (see also Petitjean & Srianand 1999; Srianand &
Petitjean 2000).
It can be seen in Fig. 6 that absorption lines from low-ionization
species (C II, Si II and Al II) are present in a well
defined narrow component at
= 2.0819. The presence of
strong associated Si II* and C II* lines suggests either that the electron
density of the gas is large or that the gas is very close to an IR emitting
source.
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Figure 9: Voigt profile fits to the Al III doublets. The observed (solid line) and model profiles for complete coverage (dotted line) and with 30% coverage (dashed line) are presented. |
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The observed equivalent widths and profiles of the two lines
C II
and C II*
are similar. Since
their rest wavelength and oscillator strengths (0.1278 and 0.1149
respectively) are nearly identical, C II and C II* have about the same column
densities, if the lines are not saturated.
If we assume electron collisions are responsible for the excitation, the
electron density
is then given by,
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(2) |
From the strength of Si II
and Si II*
,
at
,
we derive that the ratio
= N(Si II)/N(Si II*) is in the
range 1.58 <
< 2.36 for a covering factor in the range 0.3-1.0.
Note that the above range also includes Voigt profile fitting
errors in estimating the individual column densities. Assuming that
excitation and de-excitation are due to electron collisions we obtain
Indeed, excited levels can be populated by IR radiation emitted by
the QSOs. In that, case,
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(4) |
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(5) |
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(6) |
Therefore the dominant excitation process is probably pumping by the
infrared ambient radiation field and it is not possible to estimate
the electronic density from Eqs. (1) and (2). Srianand & Petitjean (2000)
reached a similar conclusion to explain the excitation of fine-structure
lines
in the
= 3.8931 system toward APM 08279+5255.
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Figure 10: Time variability of C IV absorption. The continuous line corresponds to our UVES data and the dotted line is the CASPEC spectrum from Lespine & Petitjean (1997). The resolution of the UVES spectrum is degraded to match that of the CASPEC data. |
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If the variations are due to changes in the optical depth, then the
variability time scale gives the recombination time scale. If the gas is
highly ionized so that
ni+1>ni, then the recombination
time scale is given by
Assuming C IV is the dominant ionization species and using the
recombination cross-section for C IV given by Aldrovandi & Péquignot (1986)
and Péquignot et al. (1991), the electron density,
,
is given by
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Figure 11: Time variability of Si II absorption lines (marked with "X''). The solid line corresponds to the UVES data and the dotted line is the CASPEC data from Lespine & Petitjean (1997). |
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Figure 12: Time variability of the covering factor of the C IV absorption lines. The solid line corresponds to the UVES data and the dotted line is the CASPEC spectrum from Lespine & Petitjean (1997). |
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The comparison of covering factors estimated at two epochs (see
Fig. 12) suggests that there could be some variation from one
epoch to the other. However the S/N ratio in our CASPEC spectrum,
10, implies an error of up to 0.1 in the covering factor
determination. Within this uncertainty we cannot ascertain the variation
in the covering factor between the two epochs. Also there is no
statistically significant difference in the covering factor of C IV absorption between UVES data and MMT data of Dinshaw & Impey (1996).
It is possible that the relative increase in the C IV column density
between years 1994 and 2000,
1.2, corresponds to a change
of the C IV/C ratio and therefore a change in the ionization parameter.
From the models by Hamann (1997) we derive that the gas has an ionization
parameter log U of the order of -1 and that the increase in
N(C IV) corresponds to a decrease of the ionization parameter by a
factor larger than 2.
This cannot be due to changes in the ionizing flux from the quasar as a change
by
1 mag would have been noticed. It is also difficult to imagine that
the distance of the cloud from the central ionizing source has increased by a
factor 1.4. Thus the observed variation in the C IV profile could be
either due to some non-equilibrium process or due to changes in the
internal dynamics of the cloud. In order to understand the origin
of the variability it is important to have a high resolution spectroscopic
monitoring of this system.
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Figure 13:
Profile of the Lyman- |
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Figure 14:
Absorption profiles of some of the standard
absorption lines in the
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The Mg II
2797 absorption profile shows a strong
component with narrow and weak satellites (marked with vertical dotted
lines in Fig. 14) seen on both sides and spreading in total
430 km s-1. This is a typical characteristic of the intervening
Mg II systems. Interestingly, some of the narrow components
exhibit Si II, C II and Fe II absorption lines
with weak associated absorption lines of Si IV and C IV.
When weaker transitions are considered, the strong feature splits into two
main components of similar characteristics at
= 2.1390 and
2.1394 (marked with dashed vertical lines in Fig. 14).
There are absorption lines at the expected positions of Fe
III
and Si III
.
As these lines
could be blended with intervening Lyman-
absorption lines,
we
derive upper limits on the corresponding column densities.
The two strong components show detectable absorption from
C I, N I, P II, Mg I, Mg II, S II,
Ni II, Zn II, Cr II
(see Fig. 15).
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Figure 15:
Absorption profiles of few transitions in the
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Based on the absence of absorption from molecular hydrogen in the Lyman-band,
we derive an upper limit of 1014 cm-2 for the 2 column
density in both components and therefore, the molecular fraction
f = 2N(H2)/(2N(H2) + N(H I))
.
As shown by Petitjean et al. (2000), such low value is probably consequence
of high temperature (T > 3000 K) in diffuse gas.
We estimate the upper limit on N(C I*) using a combined
spectrum obtained by stacking the regions centered at rest
wavelengths 1277.28, 1277.51, 1329.08, 1329.10, 1329.12, 1560.68,
1560.71, 1656.26, 1657.38 and 1657.91 Å. There are coincident
absorption features at the expected position of C II* for
both components at
= 2.1390 and 2.1394 (see Fig 14).
The C II* absorption at
= 2.1390 is probably (at
least partly) blended with C II
1334 from a
narrow component at 258 km s-1 seen in Mg II. The C II*
absorption at
= 2.1394 has two sub-components. The red one
is blended with C II
1334 at 323 km s-1, the other one at
= 2.1394 is free of blending. From the fact that the
C II
line is saturated we obtain a lower limit
N(C II) > 3
cm-2.
| Species |
|
|
[X/H] |
| H I |
|
||
| H2 | <1014 | ||
| C I |
|
|
|
| C I* | |||
| C II* | ..... |
|
|
| C II | |||
| N I |
|
|
-1.66 |
| O I | >
|
|
>-0.64 |
| Mg I |
|
|
|
| Mg II |
|
+0.05 | |
| Si II |
|
|
-0.02 |
| P II |
|
|
-0.03 |
| S II |
|
|
-0.15 |
| S III | |||
| Cr II |
|
|
-0.53 |
| Cr III | |||
| Mn II |
|
|
-0.75 |
| Fe II |
|
|
-0.65 |
| Fe III | |||
| Ni II |
|
|
-0.56 |
| Zn II |
|
|
-0.26 |
| [X/H] = log (N(X)/N(H)]-log(N(X)/N(H)) |
|||
Before discussing the chemical composition of the gas, one has to worry
about potential ionization corections especially for a cloud with
log N(H I)
19.7. From Table 1, it can be seen that
N(Cr III)/N(Cr II) < 0.77 and 0.63 and
N(Fe III)/N(Fe II) < 1.7 and 0.42 in the two components
respectively. As the two components have otherwise similar characteristics,
we can conclude that most of the metals are in the singly ionized state.
Howk & Sembach (1999) have shown that if
N(Fe III)/N(Fe II) < 1, the ionization correction for
relative metallicity is negligible for all species of interest here.
Absolute metallicities could be slightly underestimated but by no more
than a factor of two.
Zinc metallicity is of the order of 0.5 solar. The consistent and mild
depletion (of about a factor of two) of Fe, Cr and Ni compared to Zn
is suggestive of small amounts of dust if any. The four
-elements Mg,
Si, P, and S have consistent metallicities slightly larger (by
about a factor of two) than the Zn metallicity. Note however that
sulphur has slightly smaller metallicity compared to the other
-elements. Given the uncertainties involved in
nucleosynthesis models, it is difficult, if not impossible, to draw
any conclusion from one measurement. However it is interesting
to note that such an abundance pattern is commonly seen in damped
Lyman-
systems (see e.g. Lu et al. 1996) apart from the fact that
the system toward Tol 1037-2703 is the damped system of highest metallicity
at such redshift. In addition, the nitrogen abundance is quite small,
[N/Zn] = -1.3, [N/S] = -1.5.
This is broadly consistent with nitrogen being produced as a secondary
element in massive stars with little contribution from the primary production
that occurs in intermediate mass stars (3-8
). If true,
this means the star formation in this system was intense and has proceeded
very quickly through the formation of massive stars.
However, it is surprizing to find such low [N/Zn] = -1.3 ratio
when [Zn/H] = -0.3 (see e.g. Centurion et al. 1998).
Note that H I and N I are tied up by charge exchange reaction.
Although one can question the charge exchange reaction rate
between hydrogen and nitrogen, especially if the temperature of the gas
is high, it seems difficult to explain the low N I/H I ratio by
ionization effects only (see also Viegas 1995). Finally, it is most
interesting to note that the abundance pattern in the
= 2.139
system is close to what is observed in the Magellanic Bridge (Lehner et al.
2001) whereas the column densities are similar to those in the
Weak Low Velocity (WLV) gas toward 23 Orionis (see Welty et al. 1999) except
for N I which is much stronger toward 23 Ori.
This could suggest again that this damped Lyman-
system arises
in halo-like gas rather than through a typical galaxy disk.
Assuming that the carbon abundance is similar to that of silicon and that
C II is the dominant ionization state we derive a conservative upper
limit on the C II column density to be 1.6
in the
= 2.1394 component. Using the measured column density of
C II* and assuming collisional excitation and radiative deexcitation
of the fine-structure level we determine a range of electron density,
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(10) |
![]() |
(11) |
Similarly from Mg I and Mg II column densities, we obtain
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(12) |
It is known that the fine structure lines of C I can be excited by the
cosmic microwave background radiation (Bahcall & Wolf 1968; Meyer et al.
1986) and therefore can be used to constrain its temperature. Assuming the
CMBR pumping to be the only excitation mechanism we obtain an upper limit on
the temperature of the background to be 16.4 and 13.2 K for
= 2.1390
and 2.1394 components respectively (see Srianand et al. 2000 for details on
the derivation). These limits are consistent with the value of 8.6 K
expected in the framework of standard hot Big-Bang cosmology.
We show, using C IV and Al III doublets, that the gas responsible for
the
= 2.082 system does not cover the background source of continuum
completely. Spectra of Tol 1037-2703 obtained at two different
epochs, separated by
2 yrs in the rest frame of the QSO, suggests
variability of the C IV absorption. The relative strength of
the fine-structure lines due to Si II and C II is a consequence of excitation
by a strong IR source, probably associated with the quasar.
Similar properties have been derived in the case of the
= 3.8931
system toward APM 08279+5255 (Srianand & Petitjean 2000).
We note that the covering factor for C IV,
0.86, is
constant over the velocity range span by the absorption line. The covering
factor estimated for Al III,
0.3, is much less,
confirming the findings by Petitjean & Srianand (1999) that the covering
factor is increasing with increasing ionization state.
We report the detection of weak low-ionization lines such as C I,
Zn II, Cr II, Ni II, P II and S II
in the moderately damped (log N(H I) = 19.7)
2.139 system.
These lines are detected in two
components at
2.1390 and 2.1394. The absolute metallicity is
close to solar with [Zn/H] = -0.26. The
-chain elements have
metallicities consistently solar (respectively +0.05, -0.02, -0.03
and -0.15 for [Mg/H], [Si/H], [P/H] and [S/H]) and iron peak
elements are depleted by a factor of about two ([Fe/Zn], [Cr/Zn],
[Mn/Zn] and [Ni/Zn] are equal to -0.39, -0.27, -0.49,
-0.30). It is noticeable that the pattern is similar to what is seen
in standard damped Lyman-
systems (Lu et al. 1996). However,
in the case of Tol 1037-2703, not only is the metallicity high but
also the nitrogen abundance is small, [N/Zn] = -1.40, which is
difficult to understand in standard nucleosynthesis models.
Such a metallicity pattern is seen, however, in the Magellanic Bridge
(Lehner et al. 2001). This clearly indicates that the period of
intense star formation activity in this system has lasted for less than
0.5 Gyr and that metals have primarily been produced by massive stars.
Using the C II* column density and the Mg I/Mg II and
C I/C II ratios, we show that the required photo-ionization rates
are higher than expected if the gas is ionized by the UV background
and some extra source of ionization is needed. Assuming that the QSO is
the ionizing source implies that the absorbing gas is situated
few Mpc away from it. The high metal enrichment, within a few Mpc from
a QSO that, in addition, shows a large variety of outflowing gas might
suggest an association of this gas with the QSO. It is possible that
this absorbing gas has in common with the quasar a period of intense star
formation and/or has been ejected from the QSO a few 108 yrs ago.
Using the limits on the C I* column density and assuming excitation is due to CMBR photons we obtain an upper limit on the temperature of the cosmic microwave background of 16.2 and 13.2 K respectively for these components. These limits are consistent with the expected temperature of 8.6 K in the framework of standard hot Big-bang cosmology.
Acknowledgements
We thank Cédric Ledoux for a careful reduction of the spectrum and Chris Impey for sharing with us a 1994 MMT spectrum. We gratefully acknowledge support from the Indo-French Centre for the Promotion of Advanced Research (Centre Franco-Indien pour la Promotion de la Recherche Avancée) under contract No. 1710-1. RS thanks IAP for hospitality during the time part of this work was completed.